Advances in Earth Science ›› 2017, Vol. 32 ›› Issue (9): 919-925. doi: 10.11867/j.issn.1001-8166.2017.09.0789

Special Issue: 青藏高原研究——青藏科考虚拟专刊

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Research Status and Prospect of the Interaction Between Tibetan Plateau Shear Line and Tibetan Plateau Vortex

Li Guoping 1, Li Shanshan 1, Huang Chuhui 2   

  1. 1.School of Atmospheric Sciences,Chengdu University of Information Technology,Chengdu 610225,China;
    2.Sichuan Meteorological Observatory, Chengdu 610072, China
  • Received:2017-02-05 Revised:2017-06-12 Online:2017-09-20 Published:2017-09-20
  • About author:Li Guoping (1963-), male, Chongqing City, Professor. Research areas include plateau & mountain meteorology and weather
  • Supported by:
    Project supported by the National Natural Science Foundation of China “A dynamical study on the mechanism of the interaction between the Tibetan Plateau shear lines and the Tibetan Plateau vortices”(No.41675057)

Li Guoping, Li Shanshan, Huang Chuhui. Research Status and Prospect of the Interaction Between Tibetan Plateau Shear Line and Tibetan Plateau Vortex[J]. Advances in Earth Science, 2017, 32(9): 919-925.

The Tibetan Plateau Shear Line (TPSL) is usually accompanied by the Tibetan Plateau Vortex (TPV) and this phenomenon is one of the assembled weather systems over the Tibetan Plateau (TP) and its surrounding areas. This assembled system plays a very important role in the high impact weather process in the TP and East China. We reviewed the research history and progress of TPVs and TPSLs, and mainly discussed the relationship and interaction mechanism of them. According to the latest research achievement of TPSLs and its relationship with TPVs, the development and application trends of related theory and methods, we proposed several notable new research directions in the field of this study. It is not clear for the relationship and the physical mechanism of the interaction between TPSLs and TPVs as well as some high impact weather initiated by them currently. Therefore, this research work is really quite important for theoretical development of weather dynamics of the TP, and is expected to provide a theoretical guide for severe weather analysis and forecast over the TP and its neighborhood.
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